Russian Arctic Strategies and Recent Deals
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Satellite Ice Extent, Sea Surface Temperature, and Atmospheric 2 Methane Trends in the Barents and Kara Seas
The Cryosphere Discuss., https://doi.org/10.5194/tc-2018-237 Manuscript under review for journal The Cryosphere Discussion started: 22 November 2018 c Author(s) 2018. CC BY 4.0 License. 1 Satellite ice extent, sea surface temperature, and atmospheric 2 methane trends in the Barents and Kara Seas 1 2 3 2 4 3 Ira Leifer , F. Robert Chen , Thomas McClimans , Frank Muller Karger , Leonid Yurganov 1 4 Bubbleology Research International, Inc., Solvang, CA, USA 2 5 University of Southern Florida, USA 3 6 SINTEF Ocean, Trondheim, Norway 4 7 University of Maryland, Baltimore, USA 8 Correspondence to: Ira Leifer ([email protected]) 9 10 Abstract. Over a decade (2003-2015) of satellite data of sea-ice extent, sea surface temperature (SST), and methane 11 (CH4) concentrations in lower troposphere over 10 focus areas within the Barents and Kara Seas (BKS) were 12 analyzed for anomalies and trends relative to the Barents Sea. Large positive CH4 anomalies were discovered around 13 Franz Josef Land (FJL) and offshore west Novaya Zemlya in early fall. Far smaller CH4 enhancement was found 14 around Svalbard, downstream and north of known seabed seepage. SST increased in all focus areas at rates from 15 0.0018 to 0.15 °C yr-1, CH4 growth spanned 3.06 to 3.49 ppb yr-1. 16 The strongest SST increase was observed each year in the southeast Barents Sea in June due to strengthening of 17 the warm Murman Current (MC), and in the south Kara Sea in September. The southeast Barents Sea, the south 18 Kara Sea and coastal areas around FJL exhibited the strongest CH4 growth over the observation period. -
Zeszyt 10. Morza I Oceany
Uwaga: Niniejsza publikacja została opracowana według stanu na 2008 rok i nie jest aktualizowana. Zamieszczony na stronie internetowej Komisji Standaryzacji Nazw Geograficznych poza Granica- mi Rzeczypospolitej Polskiej plik PDF jest jedynie zapisem cyfrowym wydrukowanej publikacji. Wykaz zalecanych przez Komisję polskich nazw geograficznych świata (Urzędowy wykaz polskich nazw geograficznych świata), wraz z aktualizowaną na bieżąco listą zmian w tym wykazie, zamieszczo- ny jest na stronie internetowej pod adresem: http://ksng.gugik.gov.pl/wpngs.php. KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju NAZEWNICTWO GEOGRAFICZNE ŚWIATA Zeszyt 10 Morza i oceany GŁÓWNY URZĄD GEODEZJI I KARTOGRAFII Warszawa 2008 KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju Waldemar Rudnicki (przewodniczący), Andrzej Markowski (zastępca przewodniczącego), Maciej Zych (zastępca przewodniczącego), Katarzyna Przyszewska (sekretarz); członkowie: Stanisław Alexandrowicz, Andrzej Czerny, Janusz Danecki, Janusz Gołaski, Romuald Huszcza, Sabina Kacieszczenko, Dariusz Kalisiewicz, Artur Karp, Zbigniew Obidowski, Jerzy Ostrowski, Jarosław Pietrow, Jerzy Pietruszka, Andrzej Pisowicz, Ewa Wolnicz-Pawłowska, Bogusław R. Zagórski Opracowanie Kazimierz Furmańczyk Recenzent Maciej Zych Komitet Redakcyjny Andrzej Czerny, Joanna Januszek, Sabina Kacieszczenko, Dariusz Kalisiewicz, Jerzy Ostrowski, Waldemar Rudnicki, Maciej Zych Redaktor prowadzący Maciej -
Circulation in the Southwestern Part of the Kara Sea in September 2007 A
ISSN 00014370, Oceanology, 2010, Vol. 50, No. 5, pp. 643–656. © Pleiades Publishing, Inc., 2010. Original Russian Text © A.G. Zatsepin, E.G. Morozov, V.T. Paka, A.N. Demidov, A.A. Kondrashov, A.O. Korzh, V.V. Kremenetskiy, S.G. Poyarkov, D.M. Soloviev, 2010, published in Okeanologiya, 2010, Vol. 50, No. 5, pp. 683–697. MARINE PHYSICS Circulation in the Southwestern Part of the Kara Sea in September 2007 A. G. Zatsepina, E. G. Morozova, V. T. Pakab, A. N. Demidova, A. A. Kondrashovb, A. O. Korzhb, V. V. Kremenetskiya, S. G. Poyarkova, and D. M. Solovievc a Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia Email: [email protected] b Atlantic Branch of the Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia c Marine Hydrophysical Institute, National Academy of Sciences of Ukraine, Sevastopol, Ukraine Received September 16, 2009; in final form, January 2, 2010 Abstract—During cruise 54 of the R/V Akademik Mstislav Keldysh to the southwestern Kara Sea (September 6 to October 7, 2007), a large amount of hydrophysical data with unique spatial resolution was obtained on the basis of measurements using different instruments. The analysis of the data gave us the possibility to study the dynamics and hydrological structure of the southwestern Kara Sea basin. The main elements of the gen eral circulation are the following: the Yamal Current, the Eastern Novaya Zemlya Current, and the St. Anna Trough Current. All these currents are topographically controlled; they flow over the bottom slopes along the isobaths. The Yamal Current begins at the Kara Gates Strait and turns to the east as part of the cyclonic cir culation. -
A Newly Discovered Glacial Trough on the East Siberian Continental Margin
Clim. Past Discuss., doi:10.5194/cp-2017-56, 2017 Manuscript under review for journal Clim. Past Discussion started: 20 April 2017 c Author(s) 2017. CC-BY 3.0 License. De Long Trough: A newly discovered glacial trough on the East Siberian Continental Margin Matt O’Regan1,2, Jan Backman1,2, Natalia Barrientos1,2, Thomas M. Cronin3, Laura Gemery3, Nina 2,4 5 2,6 7 1,2,8 9,10 5 Kirchner , Larry A. Mayer , Johan Nilsson , Riko Noormets , Christof Pearce , Igor Semilietov , Christian Stranne1,2,5, Martin Jakobsson1,2. 1 Department of Geological Sciences, Stockholm University, Stockholm, 106 91, Sweden 2 Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden 10 3 US Geological Survey MS926A, Reston, Virginia, 20192, USA 4 Department of Physical Geography (NG), Stockholm University, SE-106 91 Stockholm, Sweden 5 Center for Coastal and Ocean Mapping, University of New Hampshire, New Hampshire 03824, USA 6 Department of Meteorology, Stockholm University, Stockholm, 106 91, Sweden 7 University Centre in Svalbard (UNIS), P O Box 156, N-9171 Longyearbyen, Svalbard 15 8 Department of Geoscience, Aarhus University, Aarhus, 8000, Denmark 9 Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences, 690041 Vladivostok, Russia 10 Tomsk National Research Polytechnic University, Tomsk, Russia Correspondence to: Matt O’Regan ([email protected]) 20 Abstract. Ice sheets extending over parts of the East Siberian continental shelf have been proposed during the last glacial period, and during the larger Pleistocene glaciations. The sparse data available over this sector of the Arctic Ocean has left the timing, extent and even existence of these ice sheets largely unresolved. -
Sea of Japan a Maritime Perspective on Indo-Pacific Security
The Long Littoral Project: Sea of Japan A Maritime Perspective on Indo-Pacific Security Michael A. McDevitt • Dmitry Gorenburg Cleared for Public Release IRP-2013-U-002322-Final February 2013 Strategic Studies is a division of CNA. This directorate conducts analyses of security policy, regional analyses, studies of political-military issues, and strategy and force assessments. CNA Strategic Studies is part of the global community of strategic studies institutes and in fact collaborates with many of them. On the ground experience is a hallmark of our regional work. Our specialists combine in-country experience, language skills, and the use of local primary-source data to produce empirically based work. All of our analysts have advanced degrees, and virtually all have lived and worked abroad. Similarly, our strategists and military/naval operations experts have either active duty experience or have served as field analysts with operating Navy and Marine Corps commands. They are skilled at anticipating the “problem after next” as well as determining measures of effectiveness to assess ongoing initiatives. A particular strength is bringing empirical methods to the evaluation of peace-time engagement and shaping activities. The Strategic Studies Division’s charter is global. In particular, our analysts have proven expertise in the following areas: The full range of Asian security issues The full range of Middle East related security issues, especially Iran and the Arabian Gulf Maritime strategy Insurgency and stabilization Future national security environment and forces European security issues, especially the Mediterranean littoral West Africa, especially the Gulf of Guinea Latin America The world’s most important navies Deterrence, arms control, missile defense and WMD proliferation The Strategic Studies Division is led by Dr. -
Radioactivity in the Arctic Seas
IAEA-TECDOC-1075 XA9949696 Radioactivity in the Arctic Seas Report for the International Arctic Seas Assessment Project (IASAP) ffl INTERNATIONAL ATOMIC ENERGY AGENCA / Y / 1JrrziZr^AA 30-16 The originating Section of this publication in the IAEA was: Radiometrics Section International Atomic Energy Agency Marine Environment Laboratory B.P. 800 MC 98012 Monaco Cedex RADIOACTIVITY IN THE ARCTIC SEAS IAEA, VIENNA, 1999 IAEA-TECDOC-1075 ISSN 1011-4289 ©IAEA, 1999 Printe IAEe th AustriAn y i d b a April 1999 FOREWORD From 199 o 1993t e Internationa6th l Atomic Energy Agency's Marine Environment Laboratory (IAEA-MEL s engage IAEA'e wa ) th n di s International Arctic Seas Assessment Project (IASAP whicn i ) h emphasi bees ha sn place criticaa n do l revie f environmentawo l conditions in the Arctic Seas. IAEA-MEe Th L programme, organize framewore th n dIASAi e th f ko P included: (i) an oceanographic and an ecological description of the Arctic Seas; provisioe th (ii )centra a f no l database facilitIASAe th r yfo P programm collectione th r efo , synthesi interpretatiod san datf nmarino n ao e radioactivit Arctie th n yi c Seas; (iii) participation in official expeditions to the Kara Sea organized by the joint Russian- Norwegian Experts Group (1992, 1993 and 1994), the Russian Academy of Sciences (1994), and the Naval Research Laboratory and Norwegian Defence Research Establishment (1995); (iv) assistance wit d n laboratorsiti han u y based radiometric measurement f curreno s t radionuclide concentrations in the Kara Sea; (v) organization of analytical quality assurance intercalibration exercises among the participating laboratories; (vi) computer modellin e potentiath f o g l dispersa f radionuclideo l s released froe mth dumped f assessmeno wast d associatee ean th f o t d radiological consequencee th f o s disposals on local, regional and global scales; (vii) in situ and laboratory based assessment of distribution coefficients (Kd) and concentration factor sArctie (CFth r c)fo environment. -
FI/18 Andersen-Et-Al.-2017-Walrus-Geneticspechora
Biological Journal of the Linnean Society, 2017, XX, 1–19. With 6 figures. Walruses (Odobenus rosmarus rosmarus) in the Pechora Sea in the context of contemporary population structure of Northeast Atlantic walruses LISELOTTE WESLEY ANDERSEN1*, MAGNUS W. JACOBSEN1, CHRISTIAN LYDERSEN2, VARVARA SEMENOVA3, ANDREI BOLTUNOV3, ERIK W. BORN4, ØYSTEIN WIIG5 and KIT M. KOVACS2 1Department of Bioscience, Aarhus University, Grenåvej 14, 8410 Rønde, Aarhus, Denmark 2Norwegian Polar Institute, Fram Centre, Postbox 6606 Langnes, N-9296 Norway 3Marine Mammal Council, Nakhimovskiy ave. 36, 117218 Moscow, Russia 4Greenland Institute of Natural Resources, Box 570, 3900 Nuuk, Greenland 5Natural History Museum, University of Oslo, P. O. Box 1172, Blindern, NO-0318 Oslo, Norway Received 23 May 2017; revised 4 July 2017; accepted for publication 5 July 2017 Identifying genetically different groups of animals, occupying specific geographical areas, is a prerequisite for con- servation and management priorities. In the present study, the genetic structure of Atlantic walruses (Odobenus rosmarus rosmarus) occupying the Pechora Sea (PEC) in the western Russian Arctic, including walruses from Svalbard–Franz Josef Land (SVA–FJL) and East Greenland (EGR) regions, was investigated using 14 microsatellites (N = 159) and mtDNA sequences (N = 212). Bayesian-based clustering analysis identified two clusters: EGR and the other Northeast Atlantic areas. Pairwise FST analyses based on microsatellites revealed low but significant genetic differences between walruses from the PEC and SVA–FJL groups, which was supported by mtDNA analysis. FST was not significant for all sampling years, indicating a temporal effect or male-biased gene flow. Extended Bayesian Skyline Plots suggested a constant female subpopulation size (Nef) for EGR and an increase for the SVA–FJL and PEC groups that commenced around 40–30 Kyr ago, indicating different demographic histories for walruses in the EGR. -
5.2 Barents Sea Ecoregion – Fisheries Overview
ICES Fisheries Overviews Barents Sea Ecoregion Published 29 November 2019 5.2 Barents Sea Ecoregion – Fisheries overview Table of contents Executive summary ...................................................................................................................................................................................... 1 Introduction .................................................................................................................................................................................................. 1 Who is fishing ............................................................................................................................................................................................... 2 Catches over time ......................................................................................................................................................................................... 6 Description of the fisheries........................................................................................................................................................................... 8 Fisheries management ............................................................................................................................................................................... 12 Status of the fishery resources .................................................................................................................................................................. -
Arctic Cephalopod Distributions and Their Associated Predatorspor 146 209..227 Kathleen Gardiner & Terry A
Arctic cephalopod distributions and their associated predatorspor_146 209..227 Kathleen Gardiner & Terry A. Dick Biological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada Keywords Abstract Arctic Ocean; Canada; cephalopods; distributions; oceanography; predators. Cephalopods are key species of the eastern Arctic marine food web, both as prey and predator. Their presence in the diets of Arctic fish, birds and mammals Correspondence illustrates their trophic importance. There has been considerable research on Terry A. Dick, Biological Sciences, University cephalopods (primarily Gonatus fabricii) from the north Atlantic and the west of Manitoba, Winnipeg, Manitoba R3T 2N2, side of Greenland, where they are considered a potential fishery and are taken Canada. E-mail: [email protected] as a by-catch. By contrast, data on the biogeography of Arctic cephalopods are doi:10.1111/j.1751-8369.2010.00146.x still incomplete. This study integrates most known locations of Arctic cepha- lopods in an attempt to locate potential areas of interest for cephalopods, and the predators that feed on them. International and national databases, museum collections, government reports, published articles and personal communica- tions were used to develop distribution maps. Species common to the Canadian Arctic include: G. fabricii, Rossia moelleri, R. palpebrosa and Bathypolypus arcticus. Cirroteuthis muelleri is abundant in the waters off Alaska, Davis Strait and Baffin Bay. Although distribution data are still incomplete, groupings of cephalopods were found in some areas that may be correlated with oceanographic variables. Understanding species distributions and their interactions within the ecosys- tem is important to the study of a warming Arctic Ocean and the selection of marine protected areas. -
Deep Structure, Tectonics and Petroleum Potential of the Western Sector of the Russian Arctic
Journal of Marine Science and Engineering Article Deep Structure, Tectonics and Petroleum Potential of the Western Sector of the Russian Arctic Alexey S. Egorov 1, Oleg M. Prischepa 2, Yury V. Nefedov 2,* , Vladimir A. Kontorovich 3 and Ilya Y. Vinokurov 4 1 The Faculty of Geology, Federal State Budget Educational Institution of Higher Education, Saint-Petersburg Mining University, 199106 Saint-Petersburg, Russia; [email protected] 2 Oil and Gas Geology Department, Federal State Budget Educational Institution of Higher Education, Saint-Petersburg Mining University, Saint-199106 Petersburg, Russia; [email protected] 3 Siberian Branch, Russian Academy of Science, The Trofimuk Institute of Petroleum Geology and Geophysics, 630090 Novosibirsk, Russia; [email protected] 4 Deep Geophysics Department, Russian Geological Research Institute, 199106 Saint-Petersburg, Russia; [email protected] * Correspondence: [email protected]; Tel.: +7-911-230-56-36 Abstract: The evolutionary-genetic method, whereby modern sedimentary basins are interpreted as end-products of a long geological evolution of a system of conjugate palaeo-basins, enables the assessment of the petroleum potential of the Western sector of the Russian Arctic. Modern basins in this region contain relics of palaeo-basins of a certain tectonotype formed in varying geodynamic regimes. Petroleum potential estimates of the Western Arctic vary broadly—from 34.7 to more than 100 billion tons of oil equivalent with the share of liquid hydrocarbons from 5.3 to 13.4 billion tons of oil equivalent. At each stage of the development of palaeo-basins, favourable geological, geochemical and thermobaric conditions have emerged and determined the processes of oil and gas formation, Citation: Egorov, A.S.; Prischepa, migration, accumulation, and subsequent redistribution between different complexes. -
Norway in Respect of Areas in the Arctic Ocean, the Barents Sea and the Norwegian Sea Executive Summary
Continental Shelf Submission of Norway in respect of areas in the Arctic Ocean, the Barents Sea and the Norwegian Sea Executive Summary 50˚00’ 85˚00’ 45˚00’ 40˚00’ 35˚00’ Continental shelf 30˚00’ 30˚00’ 200 nautical mile limit of Norway beyond 200 nautical 85˚00’ 25˚00’ 25˚00’ 20˚00’ 20˚00’ miles 15˚00’ 15˚00’ 200 nautical mile limits of other states 10˚00’5˚00’ 0˚00’ 5˚00’10˚00’ Bilateral maritime boundaries between Water depth Norway and other states 0 meter Computed median line between 500 meter Norway and the Russian Federation 1000 meter Western 80˚00’ Nansen Basin Preliminary line connecting continental 1500 meter shelf outer limit points of Norway and the Russian Federation 2000 meter Outer limit of the continental shelf 2500 meter beyond 200 nautical miles 3000 meter 2500 meter isobath 3500 meter 80˚00’ Yermak BARENTS Land boundaries between states 4000 meter Plateau Boundary between 200 nautical mile 4500 meter SEA 75˚00’ zones of Mainland Norway and around Svalbard 5000 meter 5500 meter Land Svalbard Continental shelf outer limit points Norwegian territory 60 nautical mile distance criterion Sediment thickness criterion Land, undifferentiated Knipovich Ridge Loop Greenland Hole Point of the Russian Federation 75˚00’ 70˚00’ GREENLAND SEA Bjørnøya 65˚00’ 70˚00’ Mohns Ridge Jan Mayen 60˚00’ NORWEGIAN 50˚00’ Lofoten Jan Mayen Fracture Zone SEA Basin Iceland SEAVøring Spur Jan Mayen Micro Continent Banana Hole Plateau Banana Hole 65˚00’ 45˚00’ Vøring Russian Federation Norway Plateau Basin 40˚00’ Iceland Finland 35˚00’ 60˚00’ 30˚00’ -
Appendix a Bibliographic Database – from Procite
APPENDIX A BIBLIOGRAPHIC DATABASE – FROM PROCITE Reference List 1. Alaska Department of Natural Resources: Division of Oil and Gas. Chapter Six: Specific Issues Relating to Oil and Gas Exploration, Development, Production and Transportation. Final Findings of the Director, Oil and Gas Lease Sale 87, North Slope Areawide. 1998 p. 6-5. 2. Alpha, T. R. and E, Reimnitz. Arctic Delta Processes-US Geol. Surv. 1995; Open File Report 95-843. 3. Antonov, V. S.; Ivanov, M. V., and Nalimov, Yu. V. Types of Breakup of Rivers in Siberian Arctic and Sub-Arctic Zones. The Role of Snow and Ice in Hydrology: International Association Scientific Hydrology Publications; 1972: 541-545. Notes: Proceedings of the Banff Symposia 4. ARCOP. Arctic Offshore Pipeline Design and Installation Challenges [Web Page]. 2004; Accessed 2007 Jun 13. Available at: http://www.arcop.fi/workshops/workshop4day1_4.pdf . Notes: Power Point presentation 5. Arctic Coastal Dynamics. Report of the 3rd International Workshop. Rachold, V.; Brown, J.; Solomon, S., and Sollid, J. L., Editors. University of Oslo; Oslo, Norway; 2002 Dec. 6. Arnborg, L.; Walker, H. J., and Peippo, J. Water Discharge in the Colville River, 1962. Geografiska Annaler. Series A, Physical Geography. 1966; 48(4):195-210. 7. Ashford, R. A. The Effect of Strudel Scour and Ice Gouging on the Buried Pipelines in the Beaufort Sea . Sohio Construction Company, Offshore Engineering Group. San Francisco, CA; 1982; Report #SCC-OEG-R.82.4. 8. Ashton, G. D. River and Lake Ice Engineering: Water Resources Publications; 1986; pp. 318-359. ISBN: 0-918334-59-4. 9. Atwater, S. G.